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Have you checked for charcoal? Assessment of soil condition using soil organic carbon
Author(s) -
Vyšná V.,
Dyer F.,
Maher W.,
Norris R.
Publication year - 2014
Publication title -
european journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 1351-0754
DOI - 10.1111/ejss.12125
Subject(s) - charcoal , soil carbon , topsoil , environmental science , vegetation (pathology) , soil science , soil texture , soil organic matter , soil water , chemistry , medicine , organic chemistry , pathology
Summary Soil condition is commonly assessed by using soil organic carbon ( SOC ) as an indicator; however, a large proportion of the world's soils can contain charcoal, a biologically‐inert form of organic carbon. We investigated whether the presence of charcoal in soil could lead to an inaccurate assessment of soil condition when using SOC as an indicator. We sampled topsoil in a south‐east A ustralian catchment affected by severe fires in 2003. Samples ( n = 100) were analysed for two SOC fractions: (i) total SOC (t‐ SOC , loss on ignition), which included charcoal, and (ii) biologically‐active SOC (a‐ SOC , persulphate‐oxidation), which did not contain charcoal. Using novel (boosted regression trees) and traditional (linear regression) modelling methods we compared the relative importance of abiotic (slope, aspect, elevation and soil texture) and biotic (land use and vegetation structure) factors as predictors of t‐ SOC and a‐ SOC concentration. A major difference between the two response variables was less relative importance of land use as a predictor when using t‐ SOC as a response variable. Therefore, ignoring the presence of charcoal would have led to an under‐estimation of the effect of land‐use conversion on the biologically‐available SOC fraction. The presence of charcoal has important ramifications for routine assessments of soil condition given that (i) SOC is a commonly used indicator and charcoal and biologically‐active SOC differ in their effects on soil properties, (ii) fires historically occur on a large area of land, (iii) charcoal is a long‐lasting consequence of fires and (iv) charcoal can account for a large proportion of SOC and yet be unnoticed during sample preparation.